Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3193
AuthorsZanchetta, G.* 
Drysdale, R. N.* 
Hellstrom, J. C.* 
Fallick, A. E.* 
Isola, I.* 
Gagan, M. K.* 
Pareschi, M. T.* 
TitleEnhanced rainfall in the Western Mediterranean during deposition of sapropel S1: stalagmite evidence from Corchia cave (Central Italy)
Issue DateFeb-2007
Series/Report no.3-4 / 22 (2007)
DOI10.1016/j.quascirev.2006.12.003
URIhttp://hdl.handle.net/2122/3193
Keywordsclimatic change
olocene
sapropel S1
stalagmite
Subject Classification03. Hydrosphere::03.01. General::03.01.06. Paleoceanography and paleoclimatology 
AbstractA stable isotope record from a stalagmite collected from Antro del Corchia cave (Apuan Alps, Central Italy), supported by 17 uranium-series ages, indicates enhanced regional rainfall between ca 8.9 and 7.3 kyr cal. BP at the time of sapropel S1 deposition. Within this phase, the highest rainfall occurred between 7.9 and 7.4 kyr cal. BP. Comparison with different marine and lake records, and in particular with the Soreq Cave record (Israel), suggests substantial in-phase occurrence of enhanced rainfall between the Western and Eastern Mediterranean basins. There is no convincing evidence for major climatic change at the time of the “8.2 kyr event”.
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